@Article{BertaniRossHayaCohe:2015:UnAmFl,
author = "Bertani, Thiago de Castilho and Rossetti, Dilce de F{\'a}tima and
Hayakawa, Eriscon H. and Cohen, Marcelo C. L.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Universidade Estadual
do Oeste do Paran{\'a}} and {Universidade Federal do Par{\'a}
(UFPA)}",
title = "Understanding Amazonian fluvial rias based on a Late
Pleistocene–Holocene analog",
journal = "Earth Surface Processes and Landforms",
year = "2015",
volume = "40",
number = "3",
pages = "285--292",
month = "Mar.",
keywords = "Amazonia,Madeira River,fluvial ria,Late
Pleistocene–Holocene,neotectonics.",
abstract = "Fluvial rias are elongated lakes at tributary mouths that can
reach dozens of kilometers in length, constituting one of the most
remarkable features in the Amazonian landscape. Thus far,
definitive data which documents the genesis of fluvial rias have
not been published. The main goal of this work was to integrate
morphological, sedimentological and chronological information in
order to characterize fluvial paleorias in the interfluve of the
Purus and Madeira Rivers and discuss the most likely hypothesis
for their genesis. These paleorias were first observed through
remote sensing imagery as several elongated and interconnecting
belts of open vegetation that are in sharp contact with the
surrounding dense forest. The belts are branched and form a
dendritic pattern similar to many modern drainage networks. The
sedimentary record of these belts revealed the prevalence of
sharp-based sandstones and mudstones arranged into fining-upward
successions, which are compatible with deposition within channels.
Active channel and abandoned channel deposits were recognized.
These are topped by continuous mudstones related to rapid channel
abandonment and formation of a low energy basin or ria
environment. Radiocarbon dating of these deposits recorded only
Late Pleistocene and Holocene ages ranging from 21 54722
285\ cal\ yr\ bp to
59286124\ cal\ yr\ bp. This chronology for
sediment deposition is not compatible with the hypothesis of
Amazonian rias being formed by fluvial erosion during the Last
Glaciation Maximum low sea level, with sediment accumulation
during the subsequent Holocene transgression. Instead, the studied
paleorias record previous tributaries of the Madeira River that
became abandoned as the position of this river shifted
southeastward and its interfluve tilted northward, inverting the
drainage systems. Therefore, a neotectonic origin of some
Amazonian paleorias seems most likely. This hypothesis should be
considered in further investigations aiming at understanding the
origin of numerous modern fluvial rias that typify the Amazonian
landscape.",
doi = "10.1002/esp.3629",
url = "http://dx.doi.org/10.1002/esp.3629",
issn = "0197-9337",
language = "en",
targetfile = "bertani_understanding.pdf",
urlaccessdate = "27 abr. 2024"
}